在三叠纪早期的温室气体期间,致命的高温
Yadong Sun1, Michael M Joachimski, Paul B Wignall
1State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, People's Republic of China. eeys@leeds.ac.uk
概括
全球变暖导致了波斯纪末期的大规模灭绝,随着气温的快速上升,损害了赤道生物,并阻碍了生态系统的恢复. 这一事件在纪早期对海洋和陆地生态系统产生了重大影响.
科学领域:
- 古生物学的古生物学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 全球变暖是过去生物危机的一个已知的因素.
- 波斯末期的大规模灭绝是地球历史上一个重要的事件.
研究的目的:
- 为了调查早期三叠纪时期快速升温在末波斯纪大灭绝中的作用.
- 了解这些高温对赤道生态系统和生态系统恢复的影响.
主要方法:
- 对早期三亚纪的化石记录的分析.
- 古气候重建以确定温度波动.
- 海洋和陆地种群的生态分析.
主要成果:
- 波斯纪末期的大规模灭绝与全球气温急剧上升相吻合.
- 在赤道度地区,气温对生命不利,导致石灰藻和鱼类的消失.
- 生态系统的恢复被抑制,在热量最大期间,小无脊椎动物种类占主导地位.
结论:
- 早期三叠纪时期的快速,极端的气温上升是末纪大灭绝的一个主要驱动因素.
- 高温迫使陆地植物和动物从赤道地区迁移.
- 这些热事件严重破坏并抑制了生态系统的恢复.
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